沃斯托克湖和上面的冰盖之间的水交换
1Bristol Glaciology Centre, School of Geographical Sciences, University of Bristol, UK. m.j.siegert@bristol.ac.uk
Nature
|February 25, 2000
概括
沃斯托克湖的冰下融化和结表明,冰盖和湖之间的水交换很大. 这一过程影响了冰下环境,可能支持生命.
科学领域:
- 地质物理学 地质物理学
- 冰川学的冰川学
- 天体生物学 天体生物学
背景情况:
- 沃斯托克湖是南极洲的一个200公里长的冰川湖,位于沃斯托克站的冰盖下面.
- 冰盖底部的条件提供了关于冰下湖的环境和潜在可居住性的见解.
研究的目的:
- 用空中雷达分析沃斯托克湖上方的冰盖结构.
- 了解冰下湖界面上的冰水相互作用的动态.
主要方法:
- 进行了空中60MHz雷达调查,以研究冰盖结构.
- 分析的重点是确定基底冰损失和积累的区域.
主要成果:
- 在冰水界面确定了基底冰损失和积累的明显区域.
- 湖泊的北部和西部部分发生了亚冰川融化和净冰损失.
- 大约150米的冰积累 (结) 发生在湖南部分.
结论:
- 在冰盖底部和沃斯托克湖之间发生了重要的水交换.
- 这种交换使湖泊富含气体水合物,促进沉积物沉积,并驱动湖水循环.
- 这些发现对了解冰下环境的可居住性有意义.
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